Geoarchaeological analysis reveals intact Late Pleistocene deposits in a South Carolina upland basin, demonstrating exceptional artifact preservation.
Identifying intact Late Pleistocene occupations on the South Atlantic Coastal Plain is a persistent challenge due to shallow, dynamic sedimentary settings and extensive postdepositional modification. Here, we examine the sedimentological and site-formation dynamics of the Swag site (38AL137) located in an upland basin adjacent to the Savannah River in Allendale County, South Carolina. We integrate sediment characterization, artifact fabric analysis, refit data, and optically stimulated luminescence (OSL) dating to assess vertical stability and taphonomic processes within an upland pond-margin setting. Artifact orientations do not show evidence of strong preferred alignment, and inclinations show a strong preference for flat-lying positions, consistent with limited disturbance. Refit patterns display minimal vertical movement, averaging 3.2 cm, and correspond to a dense horizon of artifacts. OSL ages (16,910 ± 1145 and 10,435 ± 715 years ago) bracket the artifact horizon, providing a broad Late Pleistocene–Early Holocene time frame within which a Clovis fluted preform was deposited. These results demonstrate that upland depressions underlain by fine-grained, poorly drained sediments can preserve minimally reworked occupations. The Swag site provides a rare example of stratigraphic integrity for Late Pleistocene deposits in the American Southeast, offering a model for identifying and evaluating stable geoarchaeological contexts in similar settings.
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